Field tests were conducted in the summer of 1995 on four state-of-the-
art temperature logging systems: an analog, electric-line, system; two
pressure and temperature recording memory tools (in-hole computer sys
tems); and a Distributed optical fibre Temperature Sensing (DTS) syste
m. The tools produced accurate, detailed, temperature versus depth and
temperature gradient versus depth logs at depths to 2 km and temperat
ures to 200 degrees C. Absolute temperature differences up to 0.4 degr
ees C were noted between tools. The computer and electric-line tools h
ave significantly better precision and resolution than the DTS, but th
e DTS has the advantage of being able to measure temperature instantan
eously throughout the hole, and would be well suited for monitoring dy
namic systems and gas-filled wells. The multiple independent logs demo
nstrate that most of the ''noise'' seen in gradient logs is due to con
vection cells, which may have dimensions several times the borehole di
ameter, and that these convection cells are currently the limiting fac
tor in resolving wellbore temperatures in most settings. (C) 1998 CNR.
Published by Elsevier Science Ltd.